Differences in shape between Plinian eruption columns and lateral blast flows on Earth and between umbrella-shaped and diffuse plumes on Jupiter's moon, Io, are discussed in terms of a generalized model for thermodynamic properties and geometry of a volcanic system. -R.A.H. US Geological Survey, Flagstaff, AZ, USA.
|Original language||English (US)|
|Number of pages||15|
|State||Published - Jan 1 1984|
ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)